INVESTIGADORES
BARREDA Viviana Dora
congresos y reuniones científicas
Título:
Major floristic trends in Patagonia during the late Paleogene-early Neogene: evidence from spores and pollen grains
Autor/es:
BARREDA, V.; PALAZZESI, L.
Lugar:
Bonn
Reunión:
Congreso; 12th International Palynological Congress; 2008
Resumen:
Patagonian vegetation faced major changes in composition, structure and
distribution during the late Paleogene-early Neogene. The fragmentation of
temperate rainforests and the expansion of sclerophyllous communities in eastern
Patagonia are the most important turnovers. Fossil pollen records suggest that
Paleogene landscapes were dominated by a Gondwanic group of families comprised
mainly by Nothofagaceae, Podocarpaceae and Araucariaceae, along with
Gunneraceae, Cunoniaceae and Proteaceae. By the Early Miocene rainforest taxa
began to decline, some species became extinct (Lagarostrobos, Microcachrys,
Nothofagus subgenus Brassospora) and others were confined to moister enclaves
(Araucariaceae, Nothofagus subgenus Fuscospora). A new vegetation type composed
by drought-tolerant plants progressively spread during the Neogene; Asteraceae
(Nassauviinae, Chuquiraga), Calyceraceae (Boopis), Fabaceae (Caesalpinea,
Anadenanthera, Prosopis), Anacardiaceae (Schinus), Poaceae, Chenopodiaceae,
Convolvulaceae (Cressa) were among the most characteristic families. Some of
them may have evolved from humid or sub humid ancestors as an adaptation to the
new conditions (Asteraceae Barnadesioideae); others may have dispersed into
eastern Patagonia from Neotropical bordering regions (Fabaceae Caesalpinoideae).
The fragmentation of the rainforest communities was probably related to major
global (cooling trend) and regional (Andean uplift) events, which would have led
to a progressive desertification of the eastern Andean region. Such conditions
allowed low trees and shrubs of Celtidaceae (Celtis), Anacardicaceae (Schinus)
and Fabaceae (Prosopis, Prosopidastrum) to grow and expand by the Late Miocene.
Many of these sclerophyllous taxa are today restricted to the seasonally dry
forests of the Chaco Domain and might have derived from these Miocene ancestors.